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Water quality in the red sea coastal waters (egypt): analysis of spatial and temporal variability

机译:红海沿岸水域(埃及)的水质:时空变化分析

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In order to provide a background picture of the water quality of the Egyptian Red Sea of hydrological and chemical parameters have been measured bimonthly in 2000. Few data are available on this area, which is apparently subjected to an increasing human impact due to recreational (swimming and diving), industrial (mainly phosphate shipping and industry) and fishing/harbor activities. The results of the present study indicate that changes int he salinity and pH were not significant with highly oxygenated seawaters. The levels of suspended solids (as total suspended matter, TSM) and chlorphyll-a (Chl-a) were generally low and showed an homogeneous distribution in the study region. The ratio of chlorophyll-a to total suspended matter concentrations increased between November and March and decreased from May to September. Chlorophyll-a was significantly correlated with transparency and total suspended matter concentrations in July, September and November. Nitrogen, phosphorus and reactive silicate concentrations were generally low, and allowed classifying the Egyptian Red Sea coastal water as oligotrophic to mesotrophic. The middle region of the study area, which was located between Safaga and Qusair displayed relatively high phosphate contents when compared with other coastal areas. The high values of N:P ratios indicate that PO_4-P is the limiting factor for phytoplankton growth in the Red Sea coastal waters, with the possible exception of the Middle region. Significant relationships were found between chlorophyll-a concentrations and nutrient levels in different sampling periods. Spatial distribution patterns of the studied variables revealed that productivity of the Red Sea coastal waters is mostly controlled by phosphate concentrations, salinity, temperature and dissolved oxygen.
机译:为了提供埃及红海水质的背景图片,2000年每两个月对水文和化学参数进行一次测量。关于该地区的数据很少,由于娱乐活动(游泳),人类受到的影响显然正在增加和潜水),工业(主要是磷酸盐运输和工业)以及渔业/港口活动。本研究的结果表明,高氧化海水对盐度和pH的影响不显着。悬浮固体(作为总悬浮物,TSM)和叶绿素-a(Chl-a)的水平通常较低,并且在研究区域内显示出均匀的分布。叶绿素-a与总悬浮物浓度之比在11月至3月之间增加,而5月至9月减少。叶绿素-a与7月,9月和11月的透明度和总悬浮物浓度显着相关。氮,磷和反应性硅酸盐的浓度通常较低,可以将埃及红海沿岸水质分为中营养型和低营养型。与其他沿海地区相比,位于萨法加(Safaga)和Qusair之间的研究区中部地区磷酸盐含量较高。 N:P比值高表明PO_4-P是红海沿海水域浮游植物生长的限制因素,可能是中部地区除外。在不同采样期间,叶绿素a浓度与养分含量之间存在显着关系。研究变量的空间分布模式表明,红海沿海水域的生产力主要由磷酸盐浓度,盐度,温度和溶解氧控制。

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